琼东南盆地深水区BSR带裂隙系统空间分布特征

于俊峰; 宋瑞有; 晁彩霞; 潘光超

doi:10.3969/j.issn.0253-4193.2020.09.008

琼东南盆地深水区BSR带裂隙系统空间分布特征

doi: 10.3969/j.issn.0253-4193.2020.09.008

1.
广东石油化工学院石油工程学院，广东茂名 525000
2.
中海石油（中国）有限公司湛江分公司，广东湛江 524057

基金项目: 广东石油化工学院科研基金（2018rc09）；国家科技重大专项（2016ZX05024-002）。

详细信息

作者简介:
于俊峰（1978—），男，辽宁省大连市人，博士，从事油气勘探研究工作。E-mail：463687670@qq.com

中图分类号: P738
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- 被引次数: 0
出版历程
- 收稿日期: 2020-02-18
- 修回日期: 2020-04-09
- 网络出版日期: 2021-04-21
- 刊出日期: 2020-09-25

Spatial distribution characteristics of fracture system in BSR zone in deep water area of the Qiongdongnan Basin

1.
College of Petroleum Engineering, Guangdong University of Petrochemical Technology, Maoming 525000, China
2.
Zhanjiang Branch of China National Offshore Oil Corpration (CNOOC) Limited, Zhanjiang 524057, China

摘要

摘要: 为解决甲烷渗漏系统末端裂隙系统空间分布规律问题，基于南海北部深水区高分辨率三维地震数据，采用可视化与相干体技术描述似海底反射层分布区裂隙空间结构与分布特征，阐述了裂隙产生的地质成因类型，讨论了裂隙与其他类型输导体系对甲烷气成藏的关系。似海底反射层界面上部空间裂隙远少于下部空间的地质结构体，使水合物成藏过程中甲烷气供大于散，对研究水合物成藏和检测甲烷气的渗漏有普遍指示作用。根据裂隙的发育规模，研究区大致可以识别出短裂隙、长裂隙、裂隙束、裂隙群(组) 4种类型，它们对流体的渗漏能力依次增强，这些裂隙在地层中往往以多类型共存的方式，或与其他地质构造共同构成渗漏系统。这些结果和认识对完善深水盆地甲烷气渗漏系统水合物成藏模式及成藏机理有广泛意义。
- 琼东南盆地 /
- 深水区 /
- 裂隙 /
- 渗漏系统 /
- 空间分布
Abstract: In order to solve the problem of spatial distribution of fracture system at the end of methane leakage system, based on the high-resolution three-dimensional seismic data in the north of South China Sea, the spatial structure and distribution characteristics of fractures in bottom simulating reflector (BSR) distribution area are described by using visualization and coherent body technology. The geological genetic types of fractures are described. The relationship between fractures and other types of transport systems on methane gas accumulation is discussed. The fractures in the upper part of BSR interface are far less than those in the lower part of BSR interface, which makes the methane gas supply larger than that in the process of hydrate accumulation. It has a general indicating role in studying hydrate accumulation and detecting methane gas leakage. According to the development scale of fractures, the study area can roughly identify four types of fractures, they are each short fractures, long fractures, fracture bundles, and fracture groups, which enhance the leakage capacity of fluids in turn. These fractures often coexist in multiple types in the stratum, or form a leakage system together with other geological structures. These results and understandings are of great significance to improve the gas hydrate accumulation model and mechanism of methane leakage system in deep-water basin.
- Qiongdongnan Basin /
- deep-water area /
- fracture /
- leakage system /
- spatial distribution

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图 1 莺琼盆地构造位置，研究区、三维地震及剖面位置

Fig. 1 Structural location of Yingqiong Basin, study area, 3D seismic and profile location

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图 2 琼东南盆地深水区过BSR剖面（位置见图1中L1）

Fig. 2 BSR section in deep water area of the Qiongdongnan Basin (see Fig.1 for the location of Line L1)

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图 3 BSR区裂隙空间分布

a. BSR上部空间裂隙滤波结构；b. BSR下部空间裂隙滤波结构

Fig. 3 Spatial distribution of fractures in the BSR area

a. BSR upper space fracture filtering structure; b. BSR lower space fracture filtering structure

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图 4 深水区海底BSR及裂隙结构（位置见图1中L2）

Fig. 4 BSR and fracture structure in deep water (See Fig.1 for the location of Line L2)

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图 5 莺歌海盆地东方1−1底辟构造翼部裂隙地震特征（剖面位置见图1中L3）

Fig. 5 Seismic characteristics of fractures in the wing of the eastern 1−1 bottom splitting structure in the Yinggehai Basin (see Fig.1 for the location of Line L3)

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图 6 长昌凹陷三维区古近纪继承性断裂隙与新近纪新生裂隙特征（剖面位置见图1中L4）

a.同构造两段两套地层的断裂体系，分别是古近纪继承性断裂，新近纪新生断裂的相干属性；b.古近纪继承性断裂地震特征；c.新近纪新生裂隙地震特征

Fig. 6 Characteristics of Paleogene inherited faults and Miocene Cenozoic fractures in the three-dimensional area of the Changchang Depression (see Fig.1 for the location of Line L4)

a. The fault system of two strata in the same structure is the coherent property of Paleogene inherited fault and Neogene new fault; b. the seismic characteristics of Paleogene inherited fault; c. the seismic characteristics of Neogene new fractures

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图 7 深水峡谷区超压裂隙及流体底辟构造（剖面位置见图1中L5）

Fig. 7 Overpressure fracture and fluid bottom splitting structure in deep water canyon area (see Fig.1 for the location of Line L5)

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图 8 琼东南盆地西南部浅水−深水区第三系压力结构

a. 单井压力回归；b.压力结构剖面

Fig. 8 Tertiary pressure structure in shallow-deep water area of the southwestern Qiongdongnan Basin

a. Single well pressure regression; b. pressure structure profile

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